Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis

Shuangshuang CHEN; Zewei WANG; Rui GAO; Yongzhang ZHOU

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Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis

Geomorphology and geological structure of South China Sea | Updated：2024-10-12

- Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis
- Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis
- 海洋湖沼学报(英文) 2023年41卷第2期页码：562-574
- Affiliations：
  
  1.School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China
  2.Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519080, China
  3.Guangdong Provincial Key Lab of Geological Processes and Mineral Resources, Guangzhou 510275, China
  4.State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361102, China
  5.Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, China
  6.State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
- Author bio：
  
  wangzw@sustech.‍edu.‍cn;
  gaorui66@mail.sysu.edu.cn
- Funds：
  
  the State Key Laboratory of Marine Environmental Science Visiting Fellowship (No. ‍MELRS2233), the State Key Laboratory of Marine Geology, Tongji University (No. ‍MGK202302), the Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (No. ‍311021003), the Zhujiang Talent Project Foundation of Guangdong Province (No. ‍2017ZT07Z066), the Fundamental Research Funds for the Central Universities, Sun Yat-sen University (Nos. ‍22qntd2101, 2021qntd23), the Major Projects of the National Natural Science Foundation of China (Nos. ‍41790465, 41590863), and the National Natural Science Foundation of China(42102333;41806077;41904045)
- DOI：
  中图分类号：
- 收稿：2021-12-15，
  
  纸质出版：2023-03-01
- Accepted：
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Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis[J]. 海洋湖沼学报(英文), 2023,41(2):562-574.

CHEN Shuangshuang,WANG Zewei,GAO Rui,et al.Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis[J].Journal of Oceanology and Limnology,2023,41(02):562-574.
Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis[J]. 海洋湖沼学报(英文), 2023,41(2):562-574. DOI：

CHEN Shuangshuang,WANG Zewei,GAO Rui,et al.Mantle sources of Cenozoic volcanoes around the South China Sea revealed by geochemical and isotopic data using the principal component analysis[J].Journal of Oceanology and Limnology,2023,41(02):562-574. DOI：

摘要

Abstract

Principal component analysis (PCA) was employed to determine the implications of geochemical and isotopic data from Cenozoic volcanic activities in the Southeast Asian region

including China (South China Sea (SCS)

Hainan Island

Fujian-Zhejiang coast

Taiwan Island)

and parts of Vietnam and Thailand. We analyzed 15 trace element indicators and 5 isotopic indicators for 623 volcanic rock samples collected from the study region. Two principal components (PCs) were extracted by PCA based on the trace elements and Sr-Nd-Pb isotopic ratios

which probably indicate an enriched oceanic island basalt-type mantle plume and a depleted mid-ocean ridge basalt-type spreading ridge. The results show that the influence of the Hainan mantle plume on younger volcanic activities (<13 Ma) is stronger than that on older ones (>13 Ma) at the same location in the Southeast Asian region. PCA was employed to verify the mantle-plume-ridge interaction model of volcanic activities beneath the expansion center of SCS and refute the hypothesis that the tension of SCS is triggered by the Hainan plume. This study reveals the efficiency and applicability of PCA in discussing mantle sources of volcanic activities; thus

PCA is a suitable research method for analyzing geochemical data.

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references

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